A micromorfologia é a ciência que permite estudar o solo e seus componentes em amostras indeformadas em uma escala microscópica permitindo identificar feições relacionados a sua formação e processos atuantes que podem ser aplicadas em estudos de gênese, física, mineralogia, microbiologia do solo, entre outros. Para que isso seja possível é necessário formar um material rígido o suficiente para ser laminado a partir de amostras indeformadas de solo, através do processo de impregnação de solo. No entanto, para esse procedimento são utilizados atualmente, resinas plásticas (e.g. poliéster e epóxi), e dentre elas a resina poliéster, pode ser consideradas tóxica à saúde humana devido a presença do monômero de estireno na composição, além disso há o risco de danos ao meio ambiente devido a produção de resíduos oriundos de materiais tóxicos. No Brasil, por exemplo, há poucos laboratórios que realizam o processo de impregnação de amostras de solos para análises micromorfológicas, provavelmente, devido a toxicidade dos reagentes. Diante da importância da técnica para a Ciência do Solo, torna-se fundamental buscar alternativas para a técnica de micromorfologia do solo, que sejam economicamente viáveis, e que assegurem a segurança de atividades que envolvam substâncias e produtos químicos, visando garantir a proteção da saúde, da vida e das condições normais do ambiente, contribuindo para um desenvolvimento sustentável sem comprometer a qualidade do produto final. Assim, o presente trabalho teve como objetivo eliminar ou substituir a utilização do monômero de estireno no processo de impregnação de solos por substâncias similares menos tóxicas ao manuseio e avaliar o uso de soluções de resina poliéster e soluções de resina epóxi com diferentes diluentes (estireno, acetona e álcool) no processo de impregnação de amostras de solo (argiloso, textura média e arenoso). Para isso, foram utilizadas 2 tipos de resinas: resina poliéster Arazyn 1.0#00, resina poliéster Arazyn 1.0#0.8 e resina Epóxi Epoxiglass 1504; e diferentes solventes, sendo estes: o monômero de estireno, acetona P.A e álcool etílico absoluto (99,5%). Os tratamentos foram avaliados tanto para confecção de blocos quanto na fabricação de lâminas delgadas. Além disso, avaliação da qualidade da impregnação na confecção dos blocos de solo foi feita a partir dos parâmetros: odor, cor, volume de material gasto, solubilidade do pigmento, polimerização e secagem, corte, número de reimpregnações e custos dos reagentes. Também foi verificado na qualidade final do produto, a quantidade de poros não impregnados e uma avaliação qualitativa das lâminas. Verificou-se que a resina poliéster arazyn 1.0#08 tendo a acetona como solvente apresentou resultados satisfatórios na impregnação de solos, na confecção de blocos polidos e lâminas delgadas, para ambos os tipos de solo estudados. Porém, não foi capaz de substituir totalmente o estireno, contudo promove uma redução significativa do uso do estireno devido a possibilidade de substituição por acetona. Por outro lado, o tratamento com resina epóxi apresenta grande limitação da qualidade das lâminas delgadas não sendo obtidos resultados satisfatórios no produto final. No entanto, pode ser considerado uma alternativa para trabalhos que analisam apenas blocos polidos, uma vez que apresentou resultados positivos, em todas as texturas de solo que foram impregnadas. / Micromorphology uses optical microscopy and associated techniques to study soil\'s components at the microscopic scale for undisturbed samples. This technique allows identification of features related to soil processes and formation that can be applied to soil\'s genesis, physics, mineralogy, microbiology, among others. To perform these analysis, it is commonly used rigid materials to produce thin sections from undisturbed soil samples by the soil impregnation process. However, the plastic resins (e.g., polyester resin) containing the styrene monomer is considered toxic for human health. In addition, the wastes production from toxic materials may pose environmental risks. In Brazil, for instance, there are few laboratories performing the impregnation process of soil samples for micromorphological analysis, probably because of the reagents toxicity. Thus, given the importance of micromorphology for Soil Science, it is critical to seek other alternatives for soil micromorphology analysis. These alternatives must be economically feasible, chemically safe, non-hazardous for human health, attending environmental compliances, and contributing to sustainable development without compromising the product quality. Consequently, our work aimed to eliminate or replace the use of styrene monomer in the soil impregnation process by similar substances less toxic to the handling and evaluate the use of polyester resin solutions and epoxy resin solutions with different diluents (styrene, acetone and alcohol) in the impregnation process of soil samples (clayey, medium and sandy texture). We conducted an investigation using two resins, as follows: Arazyn 1.0 # 00 polyester resin, Arazyn 1.0 polyester resin # 0.8 and Epoxy resin Epoxiglass 1504; and the following solvents: styrene monomer, acetone and absolute ethyl alcohol (99.5%). We evaluated both blocks confection and thin sections manufacture. We also assessed the impregnation quality during soil blocks preparation based on the following parameters: odor, color, amount of material spent, pigment solubility, polymerization and drying, cutting, number of reimpregnations, and reagent costs. Within the product quality we also evaluate the non-impregnated pores quantities besides a qualitative evaluation of the thin sections. We found the polyester resin Arazyn 1.0 # 08 (containing acetone as a solvent) had satisfactory results in the impregnation of soil samples for both block soils and thin sections using the three soil texture types. Even though this treatment significantly decreased the use of styrene due to the potential substitution for acetone, we were unable to completely replace the styrene. On the other hand, the epoxy resin demonstrated limitations regarding the thin section quality, so that the results were not satisfactory for the final product. The epoxy resin can be considered a good alternative for analyzing soil blocks solely, since it presented positive results for the three impregnated soil textures.

Soil structure influences many chemical, biological and physical processes and it is well established that organic carbon acts as a soil binding agent. However, the precise location of organic matter and carbon in relation to structural features within intact samples is unknown. The sensitivity of organic carbon to decomposition is dependent not only upon its intrinsic chemical recalcitrance, but also its location within the soil structure. Soil structure provides organic carbon with chemical and physical protection, the extent of which varies between structural units. Furthermore soil structure is transient, and is sensitive to both environmental changes and physical disturbance, therefore it is difficult to determine and quantify the impact of this dynamic entity upon the storage of organic carbon. To date the majority of research that has advanced our understanding of the role soil structure plays in the storage of organic carbon, has relied upon some form of fractionation technique to separate aggregates from the bulk soil. However this approach has its disadvantages as much of the soil structure is destroyed; clearly when studying the impact of soil structure upon organic carbon-storage it is advantageous to implement any method that minimises disturbance to the soil structure. This study entails removing intact soil samples (through the use of kubiena tins) from long-term agricultural experimental fields at Rothamsted Research, (Hertfordshire, UK) with the aim of comparing and evaluating the location of organic matter and it’s associated organic carbon, in soils with contrasting organic carbon contents and a well documented land-use history. Thin sections will be analysed by integrating conventional micromorphology, image analysis and sub-microscopy combined with microscale chemical analysis scanning electron microscopy-energy dispersive spectroscopy (SEM-EDS). In doing so a new alternative method for analysing the distribution of organic matter and organic carbon is proposed. It was found that agricultural soils, which are the same in all aspects except total-OC content, differ in total organic matter, water release characteristics, aggregate stability and pore size distribution; therefore these differences could be attributed to the relationship between OC and soil structure. The water release curve, aggregate stability and pore size distribution also differed between soils with similar OC-contents but from different land-uses. The analysis of organic matter within intact soil samples provided evidence for the redistribution of organic matter as it is decomposed within the soil structure, for instance, less decomposed organ and tissue forms were located in or near to soil pores while more decomposed amorphous forms were located within the soil matrix. Since the same pattern of redistribution was observed in both agricultural and grassland soil this is likely to be directed by soil macro and micro fauna. It is concluded that since the location of different forms of organic matter is consistent across all soil, organic matter location is not responsible for creating differences in aggregate stability between treatments. Instead the results indicate that the amount and strength of organic carbon bonds and its hydrophobic properties are responsible. Micromorphology results demonstrated an absence of defined aggregation between treatments. Despite the difficulties in the interpretation of aggregation, the results contradict theories of aggregation, which state that aggregates are formed around “fresh” organic matter and it is argued that OM will undergo substantial decomposition before it acts as core for aggregation. Initial SEM-EDS analysis, has shown that in the soil matrix adjacent to organic matter (plant/organ) fragments there is a heightened concentration of C, indicating that these fragments are acting as a source of organic carbon. Interestingly BC, which represent one of the most recalcitrant C forms is also acting as a source of C, although these initial results suggest to a lesser extent than more labile C-sources. This source of organic carbon could stimulate microbial activity thereby enhancing soil structural stability. Alternatively, the release of liable carbon into soil pores may represent one route by which labile carbon enters sub-soil horizons.

Master of Science / Department of Agronomy / Michel D. Ransom / Many soils in southeastern Kansas are characterized by high clay contents and high shrink-swell potentials. Their vertic properties and claypan characteristics cause soil management to be difficult and pose problems for agricultural, environmental, and engineering uses. Thus, collecting more information and improving our understanding of these soils is an important step towards bettering our soil management techniques. The objectives of this study were to examine the morphology, processes of soil genesis, clay mineralogy, micromorphology, and potassium fixation potential of the soils of interest and how these characteristics varied between and within individual pedons. Ten pedons expected to represent varying degrees of vertic expression were selected. Methods included the use of field descriptions, routine soil laboratory characterization, micromorphological investigations, the determination of clay mineralogy by X-ray diffraction, and the measurement of potassium fixation potential. Field morphology reflected the geologic parent materials available in the region. The fine sediments that compose these clayey soils are primarily provided by the Pennsylvanian and Permian shales and limestones underlying this region and the Flint Hills to the west. Dominant pedogenic processes currently at work are clay illuviation and shrink-swell processes. Silty, non-expansive surface soils at all but sites 6 and 7 are thought to buffer the rapid wetting and drying cycles needed for maximum vertic expression. Four of the soils were dominated by smectitic minerals in the clay fraction while the rest exhibited a more mixed mineralogy. Disruption of illuvial clay features by shrink-swell movement was evident in thin section. Striated b-fabrics dominated the micromorphology except in non-expansive surface soils. K fixation of the soil surface was found to be negative in all soils, thus K fixation potential is considered very low. In subsurface horizons, K fixation generally increased with increasing vermiculite content. In addition to limited quantities of K-fixing clay minerals, naturally high K levels limited the amount of K fixation in this study. The information presented can be used to improve our understanding and management of high clay, vertic and claypan soils in southeastern Kansas.

The applications of multispectral and morphometric image analysis to soil thin section descriptions is examined. It is shown that unsupervised classification and contrast stretching can be used to enhance and label features of interest. Morphometric measurements, allow the shape and abundance of features in thin sections to be compared and statistical relationships established. This method of analysis offers a precision beyond that which is possible using a qualitative approach. Using soil micromorphology as the main analytical technique a case study was carried out to evaluate the applicability of image analysis to an investigation of an archaeological site at Lairg in northern Scotland. The interactions of anthropogenic activity and pedogenesis since the Bronze Age is examined. The condition of the soils prior to the Bronze Age is not known because no buried soils predated this period. Evidence suggests that in freely draining situations complete podzols might have formed by this time. During the Bronze and Iron Age intensive cultivation of soils occurred with associated erosion. In areas of the site, where human activity is dated to the Post Medieval period, deepening of A horizons is apparent and the soils are maintained as Brown Podzols. In many areas where human activity stops stagnopodzols are the dominant soil type. The potential of image analysis to aid soil micromorphological descriptions is demonstrated. Contrast stretching aided a qualitative subdivision of thin section slides during the case study. Morphometric analysis confirmed a relationship between shape of voids and c/f ratios in an Iron Age buried A horizon, A PM buried A horizon and an undated deep topsoil. It is concluded that the full benefits of image analysis, when used as a routine tool to aid thin section descriptions, will only be realised when procedures become more interactive and processes can be speeded up.

Os solos coesos ocorrem por quase toda a faixa litorânea brasileira ocupada pelos Tabuleiros Costeiros, e caracterizam-se por apresentar um incremento acentuado na sua resistência, a qual causa restrições no seu preparo e no crescimento das plantas. Isso ocorre devido ao mesmo apresentar-se duro a extremamente duro, quando seco e friável quando úmido. Dentre os Estados da região nordeste que possuem uma extensa área litorânea ocupada pelos Tabuleiros está o Ceará, com mais de 10.000 km2 ocupados por solos que podem ser enquadrados dentro do contexto de solos coesos. Com isso levantou-se a hipótese de que os solos coesos do Estado do Ceará apresentam as mesmas restrições físicas e químicas encontradas em outros solos pertencentes aos Tabuleiros Costeiros. O objetivo geral desta tese foi identificar a ocorrência de solos coesos no Estado do Ceará, bem como, avaliar o seu comportamento através do uso de atributos morfológicos, físicos, micromorfológicos e análise de imagens. Para alcançar o objetivo geral foram estabelecidos três objetivos específicos. Cada objetivo específico contemplou um trabalho e é apresentado como um capítulo desta tese. No primeiro procurou-se identificar e caracterizar a ocorrência de solos coesos no Ceará, usando atributos morfológicos, químicos e físicos. No segundo, foi feita uma análise do comportamento de um Argissolo Acinzentado coeso através do uso de atributos físicos, especificamente: resistência tênsil (RT), resistência do solo à penetração (RP), densidade do solo (Ds) e distribuição da porosidade total (PT). No terceiro e último trabalho realizou-se um detalhamento microscópico dos solos estudados, dando ênfase à distribuição, tamanho e orientação dos poros nas áreas adensadas e abertas (menos adensadas) do horizonte coeso, através do uso da análise de imagens. Os resultados do primeiro trabalho mostraram que os horizontes coesos encontrados no Ceará, apresentam-se semelhantes aos horizontes coesos encontrados em outros Estados brasileiros. Os resultados referentes ao segundo trabalho evidenciaram que os valores de RT, RP e Ds, mostraram-se mais elevados no solo coeso do Ceará, do que em outras áreas de Tabuleiros Costeiros estudadas no Brasil. No terceiro trabalho foi observado que o adensamento natural existente nos horizontes coesos do Ceará, além de influenciar a quantidade de poros, também influencia o seu formato e a sua orientação, e que as áreas adensadas, medidas por análise de imagem, foram os principais fatores que influenciaram o espaço poroso do solo, sendo responsável pelo aumento na resistência do solo. / The hardsetting soils may be found for almost the whole Brazilian coastal area of the Coastal Tablelands. They are characterized by presenting an accentuated increment in their mechanical resistance, which causes restrictions in the soil preparation and in the plants growth. These happen due to hardsetting soils become hard to extremely hard when dry, and crumbly when humid. Ceara is one of the northeast States that possess an extensive coastal area of Coastal Tablelands, with more than 10.000 km2 of hardsetting soils. Taking this into account, it was hypothesized that hardsetting soils of Ceara State had the same physical and chemical restrictions identified in hardsetting soils in other of Coastal Tablelands. The general objective of this thesis was to identify the occurrence of hardsetting soils in the Ceara State as well as to evaluate their behavior by using the morphological, physical, and micromorphological attributes, and image analysis. To accomplish the general objective three specific objectives were established. Each specific objective led to the accomplishment of one research, and is presented as a chapter of this thesis. In the first research was identified and characterized the occurrence of hardsetting soils in Ceara by using morphologic, chemical and physical attributes. In the second research, it was studied the behavior of a hardsetting Gray Argisol by using soil physical attributes, specifically: tensile strength (RT), soil resistance to penetration (RP), soil bulk density (Ds), and pore size distribution (PT). In the last research, the soil micromorphological features were studied, giving emphasis to the distribution, size and orientation of the pores in the more denser and less denser areas of the hardsetting horizon, by using image analysis. The results of the first research showed that the hardsetting horizons found in Ceara are similar to the hardsetting horizons found in other Brazilian States. The results regarding the second research indicated that the RT, RP and Ds values were higher in the hardsetting soil of Ceara than those measured in other hardsetting soils of the Coastal Tablelands. In the third research was observed that the existent natural compaction in the hardsetting horizons of Ceara influences the amount of pores as well as their shape and orientation, and that the denser areas, measured by image analysis, were the main factor that influenced the soil porosity, being responsible for the increase in the soil mechanical resistance.

Os solos coesos ocorrem por quase toda a faixa litorânea brasileira ocupada pelos Tabuleiros Costeiros, e caracterizam-se por apresentar um incremento acentuado na sua resistência, a qual causa restrições no seu preparo e no crescimento das plantas. Isso ocorre devido ao mesmo apresentar-se duro a extremamente duro, quando seco e friável quando úmido. Dentre os Estados da região nordeste que possuem uma extensa área litorânea ocupada pelos Tabuleiros está o Ceará, com mais de 10.000 km2 ocupados por solos que podem ser enquadrados dentro do contexto de solos coesos. Com isso levantou-se a hipótese de que os solos coesos do Estado do Ceará apresentam as mesmas restrições físicas e químicas encontradas em outros solos pertencentes aos Tabuleiros Costeiros. O objetivo geral desta tese foi identificar a ocorrência de solos coesos no Estado do Ceará, bem como, avaliar o seu comportamento através do uso de atributos morfológicos, físicos, micromorfológicos e análise de imagens. Para alcançar o objetivo geral foram estabelecidos três objetivos específicos. Cada objetivo específico contemplou um trabalho e é apresentado como um capítulo desta tese. No primeiro procurou-se identificar e caracterizar a ocorrência de solos coesos no Ceará, usando atributos morfológicos, químicos e físicos. No segundo, foi feita uma análise do comportamento de um Argissolo Acinzentado coeso através do uso de atributos físicos, especificamente: resistência tênsil (RT), resistência do solo à penetração (RP), densidade do solo (Ds) e distribuição da porosidade total (PT). No terceiro e último trabalho realizou-se um detalhamento microscópico dos solos estudados, dando ênfase à distribuição, tamanho e orientação dos poros nas áreas adensadas e abertas (menos adensadas) do horizonte coeso, através do uso da análise de imagens. Os resultados do primeiro trabalho mostraram que os horizontes coesos encontrados no Ceará, apresentam-se semelhantes aos horizontes coesos encontrados em outros Estados brasileiros. Os resultados referentes ao segundo trabalho evidenciaram que os valores de RT, RP e Ds, mostraram-se mais elevados no solo coeso do Ceará, do que em outras áreas de Tabuleiros Costeiros estudadas no Brasil. No terceiro trabalho foi observado que o adensamento natural existente nos horizontes coesos do Ceará, além de influenciar a quantidade de poros, também influencia o seu formato e a sua orientação, e que as áreas adensadas, medidas por análise de imagem, foram os principais fatores que influenciaram o espaço poroso do solo, sendo responsável pelo aumento na resistência do solo. / The hardsetting soils may be found for almost the whole Brazilian coastal area of the Coastal Tablelands. They are characterized by presenting an accentuated increment in their mechanical resistance, which causes restrictions in the soil preparation and in the plants growth. These happen due to hardsetting soils become hard to extremely hard when dry, and crumbly when humid. Ceara is one of the northeast States that possess an extensive coastal area of Coastal Tablelands, with more than 10.000 km2 of hardsetting soils. Taking this into account, it was hypothesized that hardsetting soils of Ceara State had the same physical and chemical restrictions identified in hardsetting soils in other of Coastal Tablelands. The general objective of this thesis was to identify the occurrence of hardsetting soils in the Ceara State as well as to evaluate their behavior by using the morphological, physical, and micromorphological attributes, and image analysis. To accomplish the general objective three specific objectives were established. Each specific objective led to the accomplishment of one research, and is presented as a chapter of this thesis. In the first research was identified and characterized the occurrence of hardsetting soils in Ceara by using morphologic, chemical and physical attributes. In the second research, it was studied the behavior of a hardsetting Gray Argisol by using soil physical attributes, specifically: tensile strength (RT), soil resistance to penetration (RP), soil bulk density (Ds), and pore size distribution (PT). In the last research, the soil micromorphological features were studied, giving emphasis to the distribution, size and orientation of the pores in the more denser and less denser areas of the hardsetting horizon, by using image analysis. The results of the first research showed that the hardsetting horizons found in Ceara are similar to the hardsetting horizons found in other Brazilian States. The results regarding the second research indicated that the RT, RP and Ds values were higher in the hardsetting soil of Ceara than those measured in other hardsetting soils of the Coastal Tablelands. In the third research was observed that the existent natural compaction in the hardsetting horizons of Ceara influences the amount of pores as well as their shape and orientation, and that the denser areas, measured by image analysis, were the main factor that influenced the soil porosity, being responsible for the increase in the soil mechanical resistance.

The designation of World Heritage Sites (WHS) by UNESCO is the principal international and formally recognised strategy allowing the conservation of sites of outstanding cultural value throughout the world. This study demonstrates that soils and sediments influenced by cultural activities retain cultural records (soils and sediments-based cultural records, hereafter abbreviated to SSBCR) associated with WHS, and further the understanding and contribute to the cultural value of WHS. Considering The Heart of Neolithic Orkney WHS and its surrounding landscape as the study location, systematic fieldwork is combined with geoarchaeological analyses including soil organic matter content, pH, particle size distribution, phosphorus concentration, soil magnetism and thin section micromorphology to determine the nature of the SSBCR. Chronologies of the formation of SSBCR and of palaeo-environmental records were ascertained using radiocarbon analyses and optically stimulated luminescence analysis. Findings of particular importance to the interpretation of the WHS are the identification of a Late Neolithic SSBCR located between the WHS monuments. This SSBCR is a valuable cultural record of a specific Late Neolithic community and provides significant insight into the interaction between settlement and ritual aspects of the Orcadian Late Neolithic. An understanding of these interactions is of crucial importance to a fuller interpretation of the WHS and to the wider discussion of the Orcadian Neolithic. The implications of this research to other WHS designated for their cultural value are discussed, together with future conservation considerations for this specific WHS.

This thesis offers the first detailed palaeoenvironmental analysis of wetland areas within sub-Arctic enclosed homefield’s. Significance of meadows were previously mentioned only briefly in the literature, suggesting influences in settlement site selection as well as importance in quality fodder production, producing up to two thirds of total hay resources in a somewhat marginal agricultural landscape. Given the importance of hay resources in Iceland it seems unusual these areas have received so little attention to date, despite extensive research on all other aspects of the Norse farm system. The organic sediments within the meadows, given their development in-situ over extended time periods, have the ability to record aspects of the intimate relationship between societal and environmental change, and so in a robust and holistic way our methods set integrates radiocarbon measurement, tephrochronology, palynology and thin section micromorphology from the same core; reflecting these findings against existing paleoclimate and archaeological site data. This combined application of the core techniques – palynology and soil micromorphology, has proven successful in creating effective human ecodynamic records from each of the study farms. Records obtained from the three farm sites in northwest and northern Iceland exposed the varying importance and differing utilisation of these wetland areas. Meadows would appear to have played an import role in choice of settlement site across northern Iceland, through the provision of open areas, and additional and immediately available fodder resources at settlement, in a landscape dominated by dense scrub. Meadows were found to have been in continuous use, albeit at varying levels of intensity, from settlement to the present day. In this respect the semi-natural resources are found to be remarkably resilient, demonstrating little alterations to their composition following severe climatic downturns, including that of the Little Ice Age, and volcanic eruption. Acting as a robust resource and safety buffer for settlements, contributing to fodder resources where reliability of other resources is jeopardised by environmental conditions. Research in the more marginal northwest peninsula provides the first evidence of artificially created wet meadows in Iceland, developed to give sustained fodder production for over-wintering livestock in an environment that inherently had a short growing season and lacked soil fertility. A further example of the nuanced land management practices adopted in the agriculturally fragile farmscapes of the Norse North Atlantic. The findings of the thesis have wider implications for understanding the emergence of resilient and sustainable communities in agriculturally marginal environments; to this end there remains many opportunities to use palaeoenvironmental research to study ecosystem responses to natural and anthropogenic stresses, giving us a better understanding of capacities to withstand future stresses.

As crostas são o resultado da degradação da estrutura superficial dos solos, favorecem a erosão e a degradação ambiental dos solos. Este estudo avaloiu a dinâmica da formação de crostas superficiais e as consequencias sobre a porosidade, condutividade hidráulica (K), retenção de água, densidade (Ds) e a rugosidade de um Argissolo Vermelho amarelo conduzido com diferentes sistemas de preparo do solo e aplicação de lâminas de chuva simulada. Avaliou-se também, através de um experimento em laboratório, os processos envolvidos na quebra dos agregados, sob chuvas simuladas. O experimento foi conduzido, nos anos de 2009 e 2010. Em parcelas de 15 x 30 m foram conduzidos os diferentes preparos do solo: preparo convencional (PC), preparo reduzido (PR) e sem preparo (SP). Dentro das parcelas instalou-se micro-parcelas de 1m x 1m, onde foram aplicadas diferentes lâminas de chuva simulada (0, 27, 54 e 80 mm) com intensidade de 80 mm h-1. Foram realizadas coletas de dados de rugosidade, medidas de K, coleta de amostras indeformadas de solo para análise da porosidade e confecção de lâminas delgadas, e também anéis cilíndricos para curva de retenção de água (CRA) e Ds do solo. No experimento de laboratório, utilizou-se dois solos (siltoso e argiloso) e duas classe de agregados (1-3 e 3-5 mm). Os agregados foram submetidos a diferentes chuvas simuladas (28mmh-1 + EC forte; 28mmh-1 + EC fraca; 90mmh-1 + EC forte; 90mmh-1 + EC fraca) e após avaliou-se o diâmetro médio ponderado dos agregados (DMP). A dinâmica da formação de crostas ocorreu de maneira diferenciada em ambos os sistemas de preparo. Nos sistemas de PC e PR a maior redução da porosidade, pelo efeito da chuva aplicada, ocorreu na camada da crosta e no sistema SP na camada da subcrosta. A camada da crosta foi responsável pela redução da porosidade e K, e aumento da Ds nos sistemas PC e PR. As maiores umidades volumétricas observadas nas CRA ocorreram no sistema de PR e as menores no PC e não demonstraram evolução entre as chuvas aplicadas. A rugosidade superficial do solo variou em função dos sistemas de preparo realizados. Os sistemas conservacionistas (PR e SP) apresentaram maior rugosidade no primeiro ano, no segundo ano a maior rugosidade foi observada no sistema SP. O PC demonstrou nos dois anos estudados a mesma tendência, em função das chuvas aplicadas, inicialmente ocorreu um aumento na rugosidade até uma chuva máxima diminuindo em seguida. No experimento em laboratório, as maiores reduções no DMP ocorreram até a lâmina de 3 e 2 mm para o solo argiloso e siltoso, respectivamente. Nas quantidades iniciais de chuva (lâminas iniciais) a intensidade foi determinante na redução do DMP, com o aumento da quantidade de chuva a energia cinética (EC) passou a influenciar a redução do DMP. A intensidade de 28 mm h-1 promoveu as maiores reduções do DMP possivelmente pelo maior tempo de exposição dos agregados ao molhamento. / The crusts are the result of degradation of the surface structure of the soil, favoring erosion and environmental degradation of soils. This study evaluated the dynamics of the develop surface crusts and its consequences on the porosity, hydraulic conductivity (K), water retention, bulk density (Ds) and the roughness of a Typic Hapludult conducted with different systems of tillage and application of sheets simulated rainfall. Was also evaluated through the an laboratory experiment, the processes involved in the breakdown of aggregates under simulated rainfall. The experiment was conducted in the years 2009 and 2010. In plots of 15 x 30 m were installed the soil tillage: conventional tillage (CT), reduced tillage (RT) and no-tillage (NT). Inside of the plots was installed micro-plots of 1m x 1m, which were applied different sheets of simulated rainfall (0, 27, 54 and 80 mm) with intensity of 80 mm h-1. Roughness data, K measurements, sampling of undisturbed soil samples for porosity analysis and preparation of thin sections, and also cylindrical rings for water retention curve (SWRC) and Ds, were collected. In the laboratory experiment two soils (Silt Loam and Clay Loam) and two aggregate classes (1-3 and 3-5 mm) were used. The aggregates were submitted to different simulated rainfall (28mmh-1 + KE strong; 28mmh-1 + KE weak; 90mmh-1 + KE strong; 90mmh-1 + KE weak) and after the mean weight diameter (MWD) was evaluated. The dynamics of crust formation occurred differently in both tillage systems. In the CT and RT systems the major reduction of the porosity, by effect of the applied rainfall, occurred in the crust layer and in the NT system occurred in the subcrosta layer. Crust formation was responsible for reducing the porosity and K, and increasing Ds, in RT and CT systems. The higher volumetric moisture contents observed in CRA occurred in the PR system and the lowest in CT. The CRA did not show changes between the applied rainfall. The surface roughness of the soil varied in relation to the tillage systems. RT and NT systems showed a higher roughness in the first year during the second year a higher roughness was observed in the NT system. The CT in the two years studied showed the same trend of evolution according to of applied rainfall, initially there was an increase in roughness up to a maximum rain and then decrease. In the laboratory experiment, the largest DMP reductions occurred in the 3 and 2 mm rainfall for the Silt Loam and Clay Loam soils, respectively. In the initial amounts of rainfall, the intensity was determinant in the MWD reduction. With the increase in the amount of rainfall, the kinetic energy influences the MWD reduction. The intensity of 28 mm h-1 produced the greatest reductions in DMP, possibly due to the longer exposure of the aggregates to wetting.

As crostas são o resultado da degradação da estrutura superficial dos solos, favorecem a erosão e a degradação ambiental dos solos. Este estudo avaloiu a dinâmica da formação de crostas superficiais e as consequencias sobre a porosidade, condutividade hidráulica (K), retenção de água, densidade (Ds) e a rugosidade de um Argissolo Vermelho amarelo conduzido com diferentes sistemas de preparo do solo e aplicação de lâminas de chuva simulada. Avaliou-se também, através de um experimento em laboratório, os processos envolvidos na quebra dos agregados, sob chuvas simuladas. O experimento foi conduzido, nos anos de 2009 e 2010. Em parcelas de 15 x 30 m foram conduzidos os diferentes preparos do solo: preparo convencional (PC), preparo reduzido (PR) e sem preparo (SP). Dentro das parcelas instalou-se micro-parcelas de 1m x 1m, onde foram aplicadas diferentes lâminas de chuva simulada (0, 27, 54 e 80 mm) com intensidade de 80 mm h-1. Foram realizadas coletas de dados de rugosidade, medidas de K, coleta de amostras indeformadas de solo para análise da porosidade e confecção de lâminas delgadas, e também anéis cilíndricos para curva de retenção de água (CRA) e Ds do solo. No experimento de laboratório, utilizou-se dois solos (siltoso e argiloso) e duas classe de agregados (1-3 e 3-5 mm). Os agregados foram submetidos a diferentes chuvas simuladas (28mmh-1 + EC forte; 28mmh-1 + EC fraca; 90mmh-1 + EC forte; 90mmh-1 + EC fraca) e após avaliou-se o diâmetro médio ponderado dos agregados (DMP). A dinâmica da formação de crostas ocorreu de maneira diferenciada em ambos os sistemas de preparo. Nos sistemas de PC e PR a maior redução da porosidade, pelo efeito da chuva aplicada, ocorreu na camada da crosta e no sistema SP na camada da subcrosta. A camada da crosta foi responsável pela redução da porosidade e K, e aumento da Ds nos sistemas PC e PR. As maiores umidades volumétricas observadas nas CRA ocorreram no sistema de PR e as menores no PC e não demonstraram evolução entre as chuvas aplicadas. A rugosidade superficial do solo variou em função dos sistemas de preparo realizados. Os sistemas conservacionistas (PR e SP) apresentaram maior rugosidade no primeiro ano, no segundo ano a maior rugosidade foi observada no sistema SP. O PC demonstrou nos dois anos estudados a mesma tendência, em função das chuvas aplicadas, inicialmente ocorreu um aumento na rugosidade até uma chuva máxima diminuindo em seguida. No experimento em laboratório, as maiores reduções no DMP ocorreram até a lâmina de 3 e 2 mm para o solo argiloso e siltoso, respectivamente. Nas quantidades iniciais de chuva (lâminas iniciais) a intensidade foi determinante na redução do DMP, com o aumento da quantidade de chuva a energia cinética (EC) passou a influenciar a redução do DMP. A intensidade de 28 mm h-1 promoveu as maiores reduções do DMP possivelmente pelo maior tempo de exposição dos agregados ao molhamento. / The crusts are the result of degradation of the surface structure of the soil, favoring erosion and environmental degradation of soils. This study evaluated the dynamics of the develop surface crusts and its consequences on the porosity, hydraulic conductivity (K), water retention, bulk density (Ds) and the roughness of a Typic Hapludult conducted with different systems of tillage and application of sheets simulated rainfall. Was also evaluated through the an laboratory experiment, the processes involved in the breakdown of aggregates under simulated rainfall. The experiment was conducted in the years 2009 and 2010. In plots of 15 x 30 m were installed the soil tillage: conventional tillage (CT), reduced tillage (RT) and no-tillage (NT). Inside of the plots was installed micro-plots of 1m x 1m, which were applied different sheets of simulated rainfall (0, 27, 54 and 80 mm) with intensity of 80 mm h-1. Roughness data, K measurements, sampling of undisturbed soil samples for porosity analysis and preparation of thin sections, and also cylindrical rings for water retention curve (SWRC) and Ds, were collected. In the laboratory experiment two soils (Silt Loam and Clay Loam) and two aggregate classes (1-3 and 3-5 mm) were used. The aggregates were submitted to different simulated rainfall (28mmh-1 + KE strong; 28mmh-1 + KE weak; 90mmh-1 + KE strong; 90mmh-1 + KE weak) and after the mean weight diameter (MWD) was evaluated. The dynamics of crust formation occurred differently in both tillage systems. In the CT and RT systems the major reduction of the porosity, by effect of the applied rainfall, occurred in the crust layer and in the NT system occurred in the subcrosta layer. Crust formation was responsible for reducing the porosity and K, and increasing Ds, in RT and CT systems. The higher volumetric moisture contents observed in CRA occurred in the PR system and the lowest in CT. The CRA did not show changes between the applied rainfall. The surface roughness of the soil varied in relation to the tillage systems. RT and NT systems showed a higher roughness in the first year during the second year a higher roughness was observed in the NT system. The CT in the two years studied showed the same trend of evolution according to of applied rainfall, initially there was an increase in roughness up to a maximum rain and then decrease. In the laboratory experiment, the largest DMP reductions occurred in the 3 and 2 mm rainfall for the Silt Loam and Clay Loam soils, respectively. In the initial amounts of rainfall, the intensity was determinant in the MWD reduction. With the increase in the amount of rainfall, the kinetic energy influences the MWD reduction. The intensity of 28 mm h-1 produced the greatest reductions in DMP, possibly due to the longer exposure of the aggregates to wetting.